Cheat Narrows & Lower Canyon

About

Cheat River, West Virginia — 1835-48 Iron Industry, Cheat Lake, Friends of the Cheat. The Cheat gathers its strength from five major tributaries known as the 'Forks of the Cheat,' all rising within the Monongahela National Forest before merging into a single current. That convergence shapes the character of the Narrows, where the river settles into a steady, accessible rhythm. The USGS gauge at 03070260 reports an average flow near 2,400 cubic feet per second, with a historical figure around 2,200; boaters look for an optimal window of roughly 1,500 to 5,000 cfs. The river drains the highest-rainfall part of West Virginia, which keeps that momentum reliable through much of the paddling season.

Long before recreation drew boaters to its corridor, the Cheat valley lay within overlapping Monongahela, Shawnee, and Lenape hunting territories. The dense mountain forests and rugged canyons made the watershed a stronghold well into the 18th century. The river's name preserves a French and English corruption of the Lenape 'Achsinwa' or 'Achsinnink,' recorded during the frontier era; some accounts instead trace 'Cheat' to the 'cheat grass' along its banks, mistaken by early settlers for edible wheat.

The watershed's defining industrial era was the 1835–1848 iron boom, when the charcoal-fired furnaces along the lower river made this the ironmaking center of the trans-Allegheny region. The industry collapsed after 1848 with the discovery of cheaper iron ore in the Lake Superior region. Timber came next: the watershed was logged from the 1830s through the 1920s to supply the regional lumber trade and the railroad expansion of the 1860s through the 1910s, worked by local sawmills, logging drives, and downstream operations. The exhaustion of old-growth stands around 1910, the start of state forestry conservation in 1915, and the establishment of state forests in the 1930s ended large-scale logging.

The river's hardest chapter came in 1994, when the T&T Mine blowout devastated the lower river with acid mine drainage and left the Cheat among the most polluted rivers in the East. Friends of the Cheat formed that year in response. Three decades of restoration have brought the river back — smallmouth bass, musky, and paddlers have all returned — and the Cheat River Festival each May is now one of the largest whitewater gatherings in the country. That recovery reflects a longer arc of study, from the first USGS surveys of the 1870s–1890s and early gauging stations through modern TMDL and restoration programs.

Today the river is broken into distinct runs. The Cheat Narrows carries paddlers from Albright to Jenkinsburg across 11 miles of Class III–IV water, offering the river's momentum without its fiercest extremes. Below it, the Cheat Canyon runs 11 classic miles from Albright to Cheat Lake at Class IV–V, threading rapids including Big Sandy, Bull Falls, and the Lower Narrows. Upstream, the Upper Cheat from Parsons to St. George runs Class II–III as a family float. The lower river ends in Cheat Lake, a 13-mile reservoir created by the 1925 Lake Lynn Dam near Morgantown. The Cheat is protected under the West Virginia Scenic Rivers Program and flanked by the Monongahela National Forest, a major tributary of the Monongahela that contributes substantially to Pittsburgh's drinking water supply.